Water in the Earth's Mantle

Review of High Pressure Science and Technology/Koatsuryoku No Kagaku To Gijutsu

Volumn 9, Issue 1, 1999, Pages 3-10

  Ono, Shigeaki ^a  

^a OKAYAMA UNIVERSITY   (Japan)

Author keywords

earth's mantle; hydrous mineral; water

Indexed keywords

EID: 33749647479     PISSN: 0917639X     EISSN: 13481940     Source Type: Journal    
DOI: 10.4131/jshpreview.9.3     Document Type: Article

References (45)

1. J. R. Delaney, D. W. Muenov and D. G. Graham: Geochim. Cosmochim. Acta., 48, 581-594 (1978), “Abundance and distribution of water, carbon and sulfur in the glassy rims of pillow basalt”.
2. C. D. Byers, M. O. Garcia and D. W. Muenov: Earth Planet. Sci. Lett., 79, 9-20 (1986), “Volatiles in basaltic glasses from the East Pacific Rise 21oN: implications for MORB sources and submarine lava flow morphology”.
3. P. J. Michael: Geochim. Cosmochim. Acta, 52, 555-566 (1988), “The concentration, behavior and storage of H2O in the suboceanic upper mantle: impHcaions for mantle metasomatism”.
4. 2 and H2O in Juan de Fuca Ridge basaltic glasses”.
5. A. Jannhon and J. L. Zimmftrmflnn- Earth Planet. Sci. Lett., 101, 323-331 (1990), “Water in oceanic basalts: evidence for dehydration of recycled crust”.
6. A. V. Sobolev and M. Chaussidon: Earth Planet. Sci. Lett., 137, 45-55 (1996), “H2O concentrations in primary melts from supra-subduction zone and mid-ocean ridges: implications for H2O storage and recycling in the mantle”.
7. R. W. T. Wilkins and W. Sabine: Am. Mineral., 58, 508-516 (1973), “Water content of some nominally anhydrous silicates”.
8. D. R. Bell and G. R. Rossman: Science, 255, 13911397 (1992), “Water in earths mantle: the role of nominally anhydrous minerals”.
9. Q. Bai and D. L. Kohlstedt: Nature 357, 672-674 (1992), “Substantial hydrogen solubility in olivine and implications for water storage in the mantle”.
10. D. L. Kohlstedt, H. Keppler, and D. C. Rubie: Contrib. Mineral. Petrol., 123, 345-357 (1996), “Solubihty of water in the a, 3 and y phases of (Mg, Fe)2Si04”.
11. T. Gasparik: J. Geophys. Res., 98, 4287-4299 (1993), “The role of volatiles in the transition zone”.
12. T. Inoue, H. Yurimoto, and Y. Kudoh: Geophys Res. Lett., 22, 117-120 (1995), “Hydous modified spinel, Mg1. 75SiH0. 5O4: a new water reservoir in the mantle transition region”.
13. L. Ackermann, L. Cemic and K. Langer: Earth. Planet. Sci. Lett., 62, 208-214 (1983). “Hydrogarnet substitution in pyrope: possible location for “water” in the mantle”.
14. R. Lu and H. Keppler: Contrib. Mineral. Petrol., 129, 35-42 (1997), “Water solubihty in pyrope to 100 kbar”.
15. B. O. Mysen and A. L. Boettcher: J. Petrol., 16, 520-548 (1975), “Melting of a hydrous mantle: I. Phase relations of natural peridotite at high pressures and temperatures with controlled activities of water, carbon dioxide, and hydrogen”.
16. Y. Nakamura and I. Kushiro: Year Book Carnegie Inst Washington, 73, 255-258 (1974), “Composition of the gas phase in Mg2Si04-Si02-H20 at 15 kbar”.
17. A. D. Shen and H. Keppler: Nature, 385, 710-712 (1997), “Direct observation of complete miscibihty in the albite-H20 system”.
18. C. T. Prewitt and L. W. Finger: in High-Pressure Research in Mineral Physics, edited by Y. Syono and M. H. Manghnani, pp. 269-274, Terra, Tokvo/AGU. Washinerton. D. C. (1992). “Crvstal chemistry of high-pressure hydrous magnesium silicates”.
19. K. Bose and J. Ganguly: Earth Planet. Sci. Lett., 136, 109-121 (1995), “Experimental and theoretical studies of the stabiHties of talc, antigorite and phase A at high pressures with applocations to subduction processes”.
20. K. Yamamoto and S.-I. Akimoto: Am. J. Sci., 277, 288-312 (1977), “The system Mg0-Si02-H20 at high pressures and temperatures-stability field for hydroxyl-chondrodite, hydroxy 1-chnohmite and 10-A phase”.
21. B. Wunder and W. Schreyer: J. Petrol., 33, 877-889 (1992), “Metastabihty of the 10-A phase in the system Mg0-Si02-H20 (MSH). What about hydrous MSH phase in subduction zone”.
22. A. E. Ringwood and A. Major: Earth Planet. Sci. Lett., 2, 130-133 (1967), “High-pressure reconnaissance investigations in the system Mg2Si04-Mg0-H20”.
23. T. Gasparik: J. Geophys. Res. 95, 15751-15769, 1990., “Phase relation in the transition zone”.
24. K. Yamamoto and S.-I. Akimoto: J. Solid State Chem., 9, 187-195 (1974), “High pressure and high temperature investigations in the system MgO-Si02-H20”.
25. L.-G. Liu: Phys. Earth Planet. Inter., 42, 255-262 (1986), “Phase transformations in serpentine at high pressures and temperatures and imphcations for subducting hthosphere”.
26. L.-G. Liu: Phys. Earth Planet. Inter., 49, 142-167 (1987), “Effects of H2O on the phase behavior of the forsterite-enstatite system at high pressures and temperatures and impUcations for the Earth”.
27. H. Yang, C. T. Prewitt, and D. J. Frost: Am. Mineral., 82, 651-654 (1997), “Crystal structure of the dense hydrous magnesium silicate, phase D”.
28. K. Kuroda and T. Irifune: in High Pressure-Temperature Research: Properties of Earth and Planetary Materials, edited by M. H. Manghnani and T. Yagi, pp. 545-554, AGU, Washington, D. C. (1998), “Observation of phase transformations in serpentine at high pressure and high temperature by in situ X ray diffraction measurements”.
29. E. Ohtani, H. Mizobata, Y. Kudoh, and T. Nagase: Geophys. Res. Lett., 22, 1047-1050 (1997), “A new hydrous sihcate, a water reservoir, in the upper part of the lower mantle”.
30. Y. Kudoh, T. Nagase, H. Mizohata, and E. Ohtani: Geophys. Res. Lett., 22, 1051-1054 (1997), “Structure and crvatal chemistrv of nhase G. a. new hydrous magnesium silicate synthesized at 22 GPa and 10500”.
31. M. Kanzaki: Phys. Earth Planet. Inter., 66, 307312 (1991), “Stability of hydrous magnesium sihcates in the mantle transition zone”.
32. D. J. Frost and Y. Fei: J. Geophys. Res., 103, 7463-7474 (1998), “Stabihty of phase D at high pressure and high temperature”.
33. W. Schreyer: J. Geophys. Res., 100, 8353-8366 (1995), “Ultradeep metamorphic rocks: the retrospective viewpoint”.
34. B. Wunder, O. Medenbach, W. Krause and W. Schreyer: Eur. J. Mineral., 5. 637-649 (1993), “Synthesis, properties and stabihty of Al3Si207 (0H)3 (phase Pi) a hydrous high-pressure phase in the system Al203-Si02-H20 (ASH)”.
35. B. Wunder, D. C. Rubie, C. R. Ross II, O. Medenbach, F. Seifert and W. Schreyer: Am. Mineral. 78, 285-297 (1993), “Synthesis, stabihty, and properties of Al2Si04 (0H)2: a fully hydrated analogue of topaz”.
36. R. A. Eggleton, J. N. Boland and A. E. Ringwood: Geochem. J., 12, 191-194 (1978), “High pressure synthesis of new alxmiinum sihcate: Al5Si50i7 (0H)”.
37. M. W. Schmidt, L. W. Finger, R. J. Angel, and R. E. Dinnebier: Am. Mineral., 83, 881-888 (1998), “Synthesis, crystal structure, and phase relations of AlSiOaOH, a high-pressure hydrous phase”.
38. M. W. Schmidt and S. Poh: Earth Planet. Sci. Lett., 124, 105-118 (1994), “The stabihty of lawsonite and zoisite at high pressures: Experiments in CASH to 92 kbar and imphcations for the presence of hydrous phases in subducted hthosphere”.
39. A. R. Pawley: Contrib. Mineral. Petrol. 118, 99108 (1994), “The pressure and temperature stabihtyhmits of lawsonite: imphcations for H2O recycling in subduction zones”.
40. M. W. Schmidt: Am. Mineral. 80, 1286-1292 (1995), “Lawsonite: upper pressure stabihty and formation of higher density hydrous phases”.
41. T. J. B. Houand, S. A. T. Redfern and A. R. Pawley: Am. Mineral., 81, 341-348 (1996), “Volume behavior of hydrous minerals at high pressure and temperature: II. Compressibihties of lawsonite, zoisite, chnozoisite, and epidote”.
42. T. Kawamoto, R. L. Hervig, and J. R. HoUoway: Earth Planet. Sci. Lett., 24, 587-592 (1996), “Experimental evidence for a hydrous transition zone in the early Earth's mantle”.
43. A. R. Pawley and J. R. HoUoway: Science 260, 664-667 (1993), “Water sources for subdution zone volcanism: new experimental constrains”.
44. S. Poh and M. W. Schmidt: J. Geophys. Res., 100, 299-314 (1995), “H2O transport and release in subduction zones: experimental constrains on basaltic and andesitic systems”.
45. S. Ono: J. Geophys. Res. 103, 18253-18267, (1998)., “Stabihty hmits of hydrous minerals in sediment and mid-ocean ridge basalt compositions: Imphcations for water transport in subduction